Mechanism of the Indian Ocean Tropical Cyclone Frequency Changes due to Global Warming - Monitoring and Prediction of Tropical Cyclones in the Indian Ocean and Climate Change - page 46

Fig. 4: CO 2 effect and SST effect on annual mean TC frequency (a, f), precipitation (b, g), upward mass flux (p-velocity at 500 hPa)
(c, h), vertical wind shear between 200 hPa and 850 hPa (d, i), and saturation deficit at 600 hPa (e, j). Each variable is averaged
over TC season of respective hemisphere (NH: Jun-Nov, SH: Jan-Apr).